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Results 21-30 of 222 (Search time: 0.156 seconds).
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21.Geochronology, geochemistry and petrogenesis of the late Palaeoproterozoic A-type granites from the Dunhuang block, SE Tarim Craton, China: implications for the break-up of the Columbia supercontinent Geochronology, geochemistry and petrogenesis of the late Paleoproterozoic A-type granite from the Dunhuang block.pdf.jpg
  Author:SHENG-YAO YU; JIAN-XIN ZHANG; XI-LIN ZHAO; JIANG-HUA GONG
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22.Zircon SHRIMP U-Pb dating of granites from Dulan and the chronological framework of the North Qaidam UHP belt, NW China Zircon SHRIMP U-Pb dating of granites from Dulan and the chronological framework of the North Qaidam UHP bel.pdf.jpg
  Author:WU CaiLai; GAO YuanHong; LI ZhaoLi; LEI Min; QIN HaiPeng; LI MinZe1
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23.High-angle fault responsible for the surface ruptures along the northern segment of the Wenchuan Earthquake Fault Zone: Evidence from the latest seismic reflection profiles High-angle Fault Responsible for the Surface Ruptures Along the Northern Segment of the Wenchuan Earthquake Fault Zone.pdf.jpg
  Author:Chan Wu; Haibing Li; Philippe Hervé Leloup; Changqing Yu; Jialiang Si; Dongliang Liu; Jiawei Pan; Marie-Luce Chevalier; Zheng Gong
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24.新疆西南天山哈布腾苏河高压-超高压变质带中 榴辉岩和蓝片岩的岩石学及变质演化 新疆西南天山低压高温变质带深熔时代及其地质意义.pdf.jpg
  Author:施建荣, 刘福来; 刘平华, 孟 恩; 刘超辉, 杨 红; 王 舫, ,蔡 佳
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25.江山—绍兴断裂带构造格局的新元古代 SHRIMP 锆石U-Pb年龄证据 江绍断裂带构造格局的新元古代U-Pb年代学依据.pdf.jpg
  Author:高林志; 张恒; 丁孝忠; 刘燕学; 张传恒; 黄志忠; 许兴苗; 周宗尧
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26.黔东地区梵净山群与下江群凝灰岩SHRIMP锆石 U-Pb年龄 黔东地区梵净山群与下江群凝灰岩SHRIMP锆石U_Pb年龄_高林志-2014.pdf.jpg
  Author:高林志; 陈建书; 戴传固; 丁孝忠; 王雪华; 刘燕学; 王敏; 张恒
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27.三饰叶肢介科 ( 犜狉犻犵犾狔狆狋犻犱犪犲犳犪犿.狀狅狏. ) 的建立及其在 叶肢介演化 、 地层划分对比上的意义 三饰叶肢介科(Triglyptidae Fam. nov.)的建立.pdf.jpg
  Author:王思恩
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28.江山--绍兴断裂带陈蔡岩群片麻岩SHRIMP锆石U--Pb年龄及其地质意义 江山-绍兴断裂带陈蔡岩群片麻岩锆石U- Pb年龄及地质意义.pdf.jpg
  Author:高林志; 丁孝忠; 刘燕学; 张传恒; 张恒; 黄志忠; 许兴苗; 周宗尧
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29.新疆准噶尔晚泥盆世法门晚期菊石动物群的发现及其意义 新疆西准噶尔晚泥盆世板海神石菊石动物群的发现及其意义.pdf.jpg
  Author:宗普; 马学平; 张美琼; 张宇波
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30.郯庐断裂山东段(胶东)中生代中酸性火山岩的锆石U-Pb年代学及地球化学特征 郯庐断裂山东段(胶东)中生代中酸性火山岩的锆石U-Pb年代学及地球化学特征.pdf.jpg
  Author:曹光跃, 薛怀民
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Results 21-30 of 222 (Search time: 0.156 seconds).